4.3 Carbon cycling Flashcards

1
Q

Autotrophs absorb CO2 from the atmosphere and convert it into

A

organic compounds.

Reduces the concentration of CO2 in the atmosphere (approximately 0.039% or 390 micromoles/mole)

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2
Q

Some CO2 will directly dissolve

A

in water (soluble), but most will combine with water to become carbonic acid.

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3
Q

Carbonic acid can dissociate to

A

form H+ and HCO3- (bicarbonate/ hydrogen carbonate)

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4
Q

H+ ions explains how carbon dioxide reduces

A

pH of water.

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5
Q

Both dissolved carbon dioxide and hydrogen carbonate ions are absorbed by

A

aquatic plants and other autotrophs that live in water.

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6
Q

Photosynthesis uses CO2 keeping the

A

concentration of CO2 inside the leaf low,
maintains concentration gradient of CO2

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7
Q

CO2 from outside the leaf diffuses down the concentration gradient into

A

the leaf

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8
Q

CO2 moves through the

A

stomatal pores in the leaves of land plants

In many aquatic plants diffusion happens directly through the surface tissues.

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9
Q

CO2 is a

A

waste product of aerobic cell respiration

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10
Q

Methanogens

A

are archaean microorganisms that produce methane as a metabolic byproduct in anaerobic respiration (methane is produced from carbon dioxide)

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11
Q

Methanogens are found in a variety of anaerobic environments:

A

Wetlands (paddies, swamps and mangroves)
Digestive tracts of animals (cows, humans, termites)
Marine & freshwater sediments (mud in lakebeds)
Landfill sites (in which organic matter has been buried)

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12
Q

Measurements indicate that the levels of atmospheric methane are

A

increasing

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13
Q

It is estimated that, on average, methane persists in the atmosphere for

A

12 years (naturally oxidized in the stratosphere)

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14
Q

The most important process of methane removal is

A

oxidation by hydroxyl radicals.
methane + hydroxyl radical → carbon dioxide + water

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15
Q

Partially decomposed organic matter can be compressed to form

A

brown soil-like peat

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16
Q

Peat is a highly effective carbon sink,

A

it is estimated that the world’s peat contains 550 Gt of carbon

it is estimated that the world’s peat contains 550 Gt of carbon

17
Q

Peat is a highly effective carbon sink,

A

it is estimated that the world’s peat contains 550 Gt of carbon

Once dried peat burns easily and can be used as a fuel.

18
Q

How does peat form?

A

Organic matter, e.g. dead leaves

Saprotrophs assimilate some carbon for growth and release as carbon dioxide during aerobic respiration.

Waterlogged soils are an anaerobic environment

saprotrophs and methanogens are inhibited

Organic matter is only partially decomposed

Partial decomposition causes acidic conditions

Large quantities of (partially decomposed) organic matter build up.

the organic matter is compressed to form peat

19
Q

There are _____________– of carbon from past geological eras

A

large deposits

20
Q

These deposits of carbon are the result of

A

incomplete decomposition of organic matter and its burial in sediment that become rock

21
Q

Coal is formed when

A

deposits of peat are buried under other sediments.
The peat is compressed and heated over millions of years eventually becoming coal.

22
Q

Oil and natural gas are formed in the

A

mud at the bottom of seas and lakes

Anaerobic conditions mean decomposition is incomplete

As mud and sediment are deposited, the partially decomposed organic matter is compressed and heated

Chemical changes produce mixtures of liquid carbon compounds or gases

Methane forms the largest part of natural gas

Deposits are mostly found in porous rocks

23
Q

Combustion

A

heated dried biomass or fossilized fuels will burn in the presence of oxygen
Fossil/Biomass fuel + O2 → CO2 + H2O

Natural forest/grass fires occur in some regions (organisms adapted to periodic fires)

Human-caused fires also occur to clear areas for agriculture or as a method of harvesting

24
Q

Some animals are composed of

A

calcium carbonate (CaCO3) structures made by secretion:
Mollusc shells
Hard corals exoskeletons

25
Q

When the animals die the soft body parts decompose, but the calcium carbonate remains to ____________ on the ocean floor (in acidic conditions CaCO3 dissolves)

A

form deposits

26
Q

The deposits are buried and eventually

A

form limestone rock.

Limestone rock is a huge carbon sink

27
Q

Imprints of the hard body parts remain in rock as

A

fossils.

28
Q

The carbon cycle explains the

A

exchange of carbon between the biosphere, lithosphere, hydrosphere, and atmosphere.

29
Q

Pool

A

reserve of C (can be organic or inorganic)

30
Q

Flux

A

transfer of C from one pool to another